Saturday, April 5, 2014

Like a giant elevator to the stratosphere


Recent research results show that an atmospheric hole over the tropical West Pacific is reinforcing ozone depletion in the polar regions and could have a significant influence on the climate of the Earth.

Potsdam, 3 April 2014. An international team of researchers headed by Potsdam scientist Dr. Markus Rex from the Alfred Wegener Institute has discovered a previously unknown atmospheric phenomenon over the South Seas. Over the tropical West Pacific there is a natural, invisible hole extending over several thousand kilometres in a layer that prevents transport of most of the natural and manmade substances into the stratosphere by virtue of its chemical composition. Like in a giant elevator, many chemical compounds emitted at the ground pass thus unfiltered through this so-called “detergent layer” of the atmosphere. Scientists call it the “OH shield”. The newly discovered phenomenon over the South Seas boosts ozone depletion in the polar regions and could have a significant influence on the future climate of the Earth – also because of rising air pollution in South East Asia.

In tropical thunderstorms over the West Pacific air masses and
the chemical substances they contain are quickly hurled upward
to the edge of the stratosphere. If there are sufficient OH
molecules in the atmosphere, the air is extensively cleaned by
chemical transformation processes. Where OH concentrations are
low, such as those now found in large sections of the tropical
West Pacific, the cleaning capacity of the atmosphere is reduced.
Photo: Markus Rex, Alfred Wegener Institute
At first Dr. Markus Rex suspected a series of flawed measurements. In October 2009 the atmospheric physicist from the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research (AWI) was on board the German research vessel “Sonne” to measure trace substances in the atmosphere in the tropical West Pacific.

Tried and tested a thousand times over, the ozone probes he sent up into the tropical sky with a research balloon every 400 kilometres reported – nothing.

Or to be more accurate: almost nothing. The ozone concentrations in his measurements remained nearly constantly below the detection limit of approx. 10 ppbv* in the entire vertical range from the surface of the Earth to an altitude of around 15 kilometres. Normally ozone concentrations in this part of the atmosphere are three to ten times higher.

Although low values at an altitude of around 15 kilometres were known from earlier measurements in the peripheral area of the tropical West Pacific, the complete absence of ozone at all heights was surprising. However, after a short period of doubt and various tests of the instruments it dawned on the worldwide recognised ozone specialist that he might be onto a phenomenon yet unknown to science. A few research years later and after the involvement of other colleagues came confirmation: Markus Rex and his team on board the “Sonne” had tracked down a giant natural hole over the tropical South Seas, situated in a special layer of the lower atmosphere known as the “OH shield”. The research results on the newly discovered OH minimum will be published soon in the journal “Atmospheric Chemistry and Physics”, with the Institute of Environmental Physics of the University of Bremen and other international research institutions as partners.
Nearly all chemical substances produced by people, animals,
plants, algae or microorganisms on the ground or in the oceans
react quickly with OH and break down in this process. During this
chemical self-cleaning process substances that are not easily
water-soluble are transformed into water-soluble products and
then washed out by precipitation. Through this mechanism OH
molecules remove most substances from the atmosphere.
The OH molecule is therefore also called the detergent of the
atmosphere. Only extremely long-lived chemical compounds,
such as methane or CFCs, also known as "ozone killers", can
rise through the OH shield into the stratosphere.
Graphics: Markus Rex, Alfred Wegener Institute
“Even though the sky appears to be an extensively uniform space for most people, it is composed of chemically and physically very different layers,” Markus Rex explains the complex makeup of the atmosphere.

The air layers near the ground contain hundreds or even thousands of chemical compounds. This is why winter and spring, mountains and sea, city and forests all have a distinct smell. The great majority of these substances are broken down into water-soluble compounds in the lower kilometres of the atmosphere and are subsequently washed out by rain.

Since these processes require the presence of a certain chemical substance, the so called hydroxyl (=OH) radical, this part of the atmosphere is called the “OH shield”. It acts like a huge atmospheric washing machine in which OH is the detergent.

The OH shield is part of the troposphere, as the lower part of the atmosphere is called. “Only a few, extremely long-lived compounds manage to make their way through the OH shield,” says Rex, “then they also get through the tropopause and enter the stratosphere.” Tropopause refers to the boundary layer between the troposphere and the next atmospheric layer above it, the stratosphere. Particularly substances that enter the stratosphere unfold a global impact. The reason for this is that once they have reached the stratosphere, their degradation products remain up there for many years and spread over the entire globe.

Extremely long-lived chemical compounds find their way to the stratosphere, even where the OH shield is intact. These include methane, nitrous oxide (“laughing gas”), halons, methyl bromide and chlorofluorocarbons (CFCs), which are notorious as “ozone killers” because they play a major role in ozone depletion in the polar regions.

Location and extent of low ozone concentrations and thus
of the OH hole over the West Pacific. Fig. (a) shows the
region of origin of the air in the stratosphere, Fig. (b) ozone
sonde measurements (dots) and satellite measurements
(coloured map) of the total amount of ozone in the
tropospheric column of air and Fig. (c) the total amount of
OH in the tropospheric column of air calculated with a model.
Graphics: Markus Rex, Alfred Wegener Institute.
After many years of research scientists now understand the complicated process of stratospheric ozone depletion very well.

“Nevertheless measured ozone depletion rates were often quite a bit larger than theoretically calculated in our models,” Markus Rex points out a long unsolved problem of atmospheric research.

“Through the discovery of the OH hole over the tropical West Pacific we have now presumably made a contribution to solving this puzzle.”

And at the same time discovered a phenomenon that raises a number of new questions for climate policy.

Researchers are now tackling these questions in a new research project funded by the EU with around 9 million euros, i.e. “StratoClim”, which is coordinated by the Alfred Wegener Institute. Within this project a new monitoring station will be established in the tropical Westpacific, together with the Institute of Environmental Physics at the University of Bremen.

“We have to realise,” reminds the Potsdam atmospheric physicist, “that chemical compounds which enter the stratosphere always have a global impact.” Thanks to the OH hole that the researchers discovered over the tropical Pacific, greater amounts of brominated hydrocarbons can reach the stratosphere than in other parts of the world. Although their ascent takes place over the tropical West Pacific, these compounds amplify ozone depletion in the polar regions. Since scientists identified this phenomenon and took it into account in the modelling of stratospheric ozone depletion, their models have corresponded excellently with the actually measured data.

However, it is not only brominated hydrocarbons that enter the stratosphere over the tropical West Pacific. “You can imagine this region as a giant elevator to the stratosphere,” states Markus Rex using an apt comparison. Other substances, too, rise here to a yet unknown extent while they are intercepted to a larger extent in the OH shield elsewhere on the globe. One example is sulphur dioxide, which has a significant impact on the climate.

Sulphur particles in the stratosphere reflect sunlight and therefore act antagonistically to atmospheric greenhouse gases like CO2, which capture the heat of the sun on the Earth. To put it simply, whereas greenhouse gases in the atmosphere heat the globe, sulphur particles in the stratosphere have a cooling effect. “South East Asia is developing rapidly in economic terms,” Markus Rex explains a problem given little attention to date. “Contrary to most industrial nations, however, little has been invested in filter technology up to now. That is why sulphur dioxide emissions are increasing substantially in this region at present.”

This is how air reaches the stratosphere. Through the rapid
upward transport in tropical thunderstorms they reach an area
of slow large-scale ascent and rise from there through the
tropopause into the stratosphere over the course of weeks.
This process is most pronounced during northern hemispheric
winter. Model calculations show that, during this season, this
process mainly takes place over the tropical West Pacific. Due
to the formation of cirrus (= ice) clouds in the extremely cold
tropical tropopause, a large portion of the water-soluble
chemical substances is removed from the air and cannot reach
the stratosphere. OH molecules transform water-insoluble into
water-soluble compounds. Hence, if the concentration of OH
molecules along the dotted transport pathways shown above
is high only few chemical compounds make it into the
stratosphere. Conversely, the lower the OH concentration is
along the transport pathways, the more chemical
compounds enter the stratosphere.
Graphics: Yves Nowak, Alfred Wegener Institute.
If one takes into account that sulphur dioxide may also reach the stratosphere via the OH hole over the tropical West Pacific, it quickly becomes obvious that the atmospheric elevator over the South Seas not only boosts ozone depletion, but may influence the climate of the entire Earth. In fact, the aerosol layer in the stratosphere, which is also composed of sulphur particles, seems to have become thicker in recent years. Researchers do not know yet whether there is a connection here.

But wouldn’t it be a stroke of luck if air pollutants from South East Asia were able to mitigate climate warming? “By no means,” Markus Rex vigorously shakes his head. “The OH hole over the South Seas is above all further evidence of how complex climate processes are. And we are still a long way off from being in a position to assess the consequences of increased sulphur input into the stratosphere. Therefore, we should make every effort to understand the processes in the atmosphere as best we can and avoid any form of conscious or unconscious manipulation that would have an unknown outcome.”

Background:

Why is there an OH hole over the West Pacific?
The air in the tropical West Pacific is extremely clean. Air masses in this area were transported across the expanse of the huge Pacific with the trade winds and for a long time no longer had contact with forests or other land ecosystems that produce innumerable short-lived hydrocarbons and release them into the air. Under these clean air conditions OH is formed from ozone through chemical transformation to a great degree. If there is hardly any ozone in the lower atmosphere (= troposphere), as is the case in the West Pacific, only little OH can be formed. The result is an OH hole.

The graph shows ozone profiles measured in three different
marine regions: the tropical Atlantic, the tropical West Pacific
and the West Pacific outside the tropics. The red curve clearly
shows that ozone is consistently very low up to an altitude of
15 kilometres over the tropical West Pacific. In the other
regions the ozone concentrations are in a range typical
for the troposphere.
Graphics: Markus Rex, Alfred Wegener Institute
Ozone, in turn, forms in the lower atmosphere only if there are sufficient nitrogen oxides there. Large amounts of nitrogen oxide compounds are produced in particular by intensive lightning over land.

However, the air masses in the tropical West Pacific were not exposed to any continental tropical storms for a very long time during their transport across the giant ocean. And the lightning activity in storms over the ocean is relatively small. At the same time the lifetime of atmospheric ozone is short due to the exceptionally warm and moist conditions in the tropical West Pacific. In this South Sea region the surface temperatures of the ocean are higher than anywhere else on our planet, which makes the air not only quite warm, but also quite moist.

The ozone is thus quickly lost, especially directly above the water. And due to the lack of nitrogen oxide compounds little ozone is subsequently formed. Rapid vertical mixing in the convection areas that exist everywhere over the warm ocean and in which the warm air rises takes care of the rest. Finally, there is no more ozone in the entire column of air in the troposphere. And without ozone (see above) the formation of OH is suppressed.

What impact does the OH hole over the West Pacific have?
The illustration shows the average lifetime of sulphur dioxide
and some brominated hydrocarbons for normal conditions
over the tropical Atlantic and for conditions of reduced
OH-concentrations over the tropical West Pacific.
Graphics: Markus Rex, Alfred Wegener Institute
The OH molecule is also called the detergent of the atmosphere. Nearly all of the thousands of different chemical substances produced by people, animals, plants, fungi, algae or microorganisms on the ground or in the oceans react quickly with OH and break down in this process. Therefore, virtually none of these substances rises into the stratosphere. In the area of the OH hole, however, a larger portion of this varied chemical mix can enter the stratosphere.

And local emissions may unfold a global impact, especially if they make it to the stratosphere. There they spread globally and can influence the composition of the air for many years – with far-reaching consequences for ozone chemistry, aerosol formation and climate.

Why wasn’t the OH hole discovered earlier?
The tropical West Pacific is one of the most remote regions on our planet. That is why extensive measurements of the air composition have yet to take place in this area. There is also a considerable gap in the otherwise dense network of global ozone measurement stations here. Even in the past measurements from the peripheral sections of the now investigated region showed minimal ozone values in the area of the upper troposphere, but not the consistently low values that have now been found across the entire depth of the troposphere. The newly discovered phenomenon reveals itself in its full scope only through the measurements that were conducted to such an extensive degree for the first time and was thus not able to be grasped at all previously.

*One part of ozone per billion by volume (ppbv) means there is one ozone molecule for every billion air molecules.

Escalating extreme weather events to hammer humanity


By Paul Beckwith

Extreme weather events are rocketing upwards in their frequency of occurrence, intensity, and duration and are impacting new regions that are unprepared. These events, such as torrential rains, are causing floods and damaging crops and infrastructure like roads, rail, pipelines, and buildings. Cities, states, and entire countries are being battered and inundated resulting in disruption to many peoples lives as well as enormous economic losses. As bad as this is, it is going to get much worse by at least 10 to 20 times. Why?

Greenhouse gas emissions from humans have changed the chemistry of the atmosphere. The optical absorption of infrared heat has increased in the atmosphere which raises temperature, and thus water vapor content, and therefore fuels more intense storms. The jet streams that guide these storms are slower and wavier and more fractured and cause our weather gyrations and weird behavior. Areas far north can get very warm, while areas far south can get very cold. Some areas get persistent drought. Then, the pattern can flip. The jet streams are much wavier in the north-south direction since the Arctic temperatures have warmed 5 to 8 times faster than the global average. This reduces the temperature difference between the Arctic and equator and basic physics forces the jets to slow and get wavier.

Why is the Arctic warming greatly amplified? The region is darkening and thus absorbing more sunlight, since the land-based snow cover in spring and the Arctic sea ice cover volume are both declining exponentially. The white snow and ice is being replaced by dark surfaces like the ocean and the tundra. The most detailed computer model on sea ice decline is a U.S. Naval Graduate School model, and it shows the sea ice cover could be gone by late summer in 2016. If this happens, the Arctic warming will rocket upwards, the jets will distort much more, and the extreme weather events will rocket upwards in frequency, amplitude, and duration and civilization will be hammered.


Paul Beckwith
Paul Beckwith is part-time professor with the laboratory for paleoclimatology and climatology, department of geography, University of Ottawa. Paul teaches climatology/meteorology and does PhD research on 'Abrupt climate change in the past and present'. Paul holds an M.Sc. in laser physics and a B.Eng. in engineering physics and reached the rank of chess master in a previous life. Below are Paul's earlier posts at the Arctic-news blog.

Tuesday, April 1, 2014

Earthquakes in the Arctic Ocean

Earthquakes in the Arctic Ocean
indications of imminent catastrophic methane eruptions?

1. Methane over Greenland

The image below shows high methane concentrations over Greenland and over the Arctic Ocean.

[ Yellow areas indicate methane readings of 1950 ppb and higher - click on image to enlarge ]
The large yellow areas on this image indicate that the methane entered the atmosphere there. This is especially likely when such large yellow areas keep appearing in the same area over a few days. In the case of the large yellow areas around Novaya Zemlya, the methane is likely to have travelled there underneath the sea ice, from the Gakkel Ridge, to enter the atmosphere where the sea ice was thin or fractured enough for the methane to pass through, as discussed in earlier posts.

As described in the post High methane readings over Greenland, huge temperature swings can hit areas over Greenland over the course of a few days. Temperature anomalies may go down as low as as -20°C one day, then climb as high as 20°C a few days later, to hit temperature anomalies as low as -20°C again some days later.

This could explain the methane over Greenland. Methane is present in the Greenland ice sheet in the form of hydrates and free gas. These huge temperature swings are causing the ice to expand and contract, thus causing difference in pressure as well as temperature. The combined shock of wild pressure and temperature swings is causing movement and fractures in the ice, and this enables methane to rise to the surface and enter the atmosphere.

To further illustrate this, the image below shows recent temperature anomaly forecasts over Greenland.

[ click on image to enlarge ]
2. What is causing these extreme weather events?

Frigid cold weather in the U.S., torrential rain and flooding in the U.K., and wild temperature swings over Greenland. What is causing these extreme weather events? 

As discussed in many previous posts, the Arctic has become warmer than it used to be and temperatures in the Arctic are rising several times faster than global temperatures. This decreases the temperature difference between the areas to the north and to the south of the Jet Stream, which in turn decreases the speed at which the Jet Stream circumnavigates the globe, making the Jet Stream more wavier and increasing opportunities for cold air to descend from the Arctic and for warm air to enter the Arctic.

3. Did temperature swings also trigger earthquakes?

[ click on image to enlarge ]
These wild temperature swings may be causing even further damage, on top of the methane eruptions from the heights of Greenland. Look at the above map, showing earthquakes that hit the Arctic in March 2014.
Topographic map of Greenland
without the Greenland Ice Sheet.

BTW, above map doesn't show all earthquakes that occurred in the Arctic Ocean in March 2014. An earthquake with a magnitude of 4.5 on the Richter scale hit the Gakkel Ridge on March 6, 2014.

Importantly, above map shows a number of earthquakes that occurred far away from faultlines, including a M4.6 earthquake that hit Baffin Bay and a M4.5 earthquake that hit the Labrador Sea. These earthquakes are unlikely to have resulted from movement in tectonic plates. Instead, temperature swings over Greenland may have triggered these events, by causing a succession of compression and expansion swings of the Greenland ice mass, which in turn caused pressure changes that were felt in the crust surrounding the Greenland Ice Sheet.

Glaciers could be the key to make this happen. Glaciers typically move smoothly and gradually. It could be, however, that such wide temperature swings are causing glaciers to come to a halt, temporarily, causing pressure to build up over a day or so, to then suddenly start moving again with a shock. Intense cold can literally freeze a glacier in its track, to be shocked into moving again as temperatures rise abruptly by 40°C or so. This can send shockwaves through the ice sheet into the crust and trigger earthquakes in areas prone to destabilization. The same mechanism could explain the high methane concentrations over the heights of Greenland and Antarctica.

Ominously, patterns of earthquakes can be indicators of bigger earthquakes yet to come.

4. Situation looks set to get a lot worse

This situation looks set to get a lot worse. Extreme weather events and wild temperature swings look set to become more likely to occur and hit Greenland with ever greater ferocity. Earthquakes could reverberate around the Arctic Ocean and destabilize methane held in the form of free gas and hydrates in sediments underneath the Arctic Ocean.

Meanwhile, as pollution clouds from North America move (due to the Coriolis Effect) over the Atlantic Ocean, the Gulf Stream continues to warm up and carry warmer water into the Arctic Ocean, further increasing the likelihood of methane eruptions from the Arctic seafloor.


The above image shows the Gulf Stream off the coast of North America, while the image below shows how the Gulf Stream continues, carrying warmer water through the Atlantic Ocean into the Arctic Ocean.


Feedbacks, such as the demise of the Arctic's snow and ice cover, further contribute to speed up the unfolding catastrophe. Methane eruptions from the seafloor of the Arctic Ocean have become especially noticeable over the past half year. The big danger is that this will develop into runaway global warming, as discussed in the recent post Feedbacks in the Arctic.

Furthermore, as-yet-unknown feedbacks may start to kick in. As an example, submarine earthquakes and volcanoes could add nutrients into the water that feed methane-producing (methanogenic) microbes. A recent study found that expansion of such microbes could have played a large role in the end-Permian extinction, and that it was catalyzed by increased availability of nickel associated with volcanism. Authors support their hypothesis with an analysis of carbon isotopic changes leading up to the extinction, phylogenetic analysis of methanogenic archaea, and measurements of nickel concentrations in South China sediments.

5. Need for comprehensive and effective action

The situation is dire and calls for comprehensive and effective action as described at the Climate Plan.




Related

- Methane Release caused by Earthquakes
http://arctic-news.blogspot.com/2013/09/methane-release-caused-by-earthquakes.html

- Seismic activity
http://arctic-news.blogspot.com/p/seismic-activity.html

- Climate Plan
https://arctic-news.blogspot.com/p/climateplan.html





Thursday, March 20, 2014

Feedbacks in the Arctic

This is more a climate report than a weather report; yet, the extreme weather that did hit the U.K. recently and that is forecast to hit large parts of North America next week may make more people realize that action is needed now. So, please share!

At the moment, a large part of Russia is experiencing temperature anomalies at the highest end of the scale, i.e. more than 36°F (20°C) warmer than average past records.


Above image shows the situation as at March 20, 2014. The image below is a forecast for March 22, 2014.


Over the past year, average temperatures over the Arctic Ocean have been much higher than they used to be, as illustrated by the NOAA image below.

Warming in the Arctic is accelerating, in part due to a number of feedbacks such as extreme weather. Temperatures over the Arctic Ocean are expected to rise even further next week. The Arctic as a whole is expected to reach average anomalies as high as 5.3°C next week, while many areas over the Arctic Ocean are expected to be hit by even higher anomalies, as the image below shows.

 [ click on image to enlarge ]
Above image also shows that, at the same time, very low temperatures - with anomalies at the low end of the scale - are expected to hit a large part of North America. The image below shows what temperatures can be expected on March 26, 2014, 12:00 UTC.


As above image illustrates, temperatures over a large part of North America can be expected to be hardly higher than temperatures over the Arctic Ocean mid next week. It is this very difference between high altitude temperatures and lower altitude temperatures that drives the Jet Stream. In the absence of much difference, changes to the Jet Stream are making it easier for cold air to move out of the Arctic and for warm air from lower latitudes to move in. The Polar Vortex is similarly affected, as illustrated by the image below.


At lower altitude, the highest wind speed detected on the image below was 94 km/h (green marker). Strong winds brought a lot of rain from the Atlantic Ocean to the U.K., as has been the case for some time.

[ click on image to enlarge ]
The result is more extreme weather, which can translate into more intense storms, heatwaves, droughts, wildfires and further havoc. Importantly, storms across the Arctic Ocean and higher wind speeds along the edges of Greenland can break up the ice and speed up its exit from the Arctic Ocean. The Naval Research Laboratory animation below shows strong winds pushing the sea ice around and speeding up its exit along the edges of Greenland. 


Despite the cold weather that has hit large parts of North America over the past few months, the water off the coast of North America has not cooled, as illustrated by the image below. The blue and lilac colored areas are in part the result of exit currents carrying cold water out of the Arctic Ocean more rapidly, while the Gulf Stream continues to carry warmer water (brown and red colored areas) into the Arctic Ocean. 

[ Sea Surface Temperatures (SST) - click on image to enlarge ]
The Arctic is especially vulnerable to warming, due to a number of circumstances, including:
- Gulf Stream carrying warmer water into the Arctic Ocean;
- Arctic snow and ice cover is at the verge of collapse;
- Methane is present in large quantities under the seafloor of the Arctic Ocean.
These circumstances and the combined impact of feedbacks such as extreme weather make that, on top of global warming, the Arctic is hit by a second, addtional kind of warming, i.e. accelerating warming in the Arctic.

The joint impact of feedbacks is becoming stronger, as temperatures keep rising in the Arctic and with continued demise of the snow and ice cover. So, let's start with feedback #1, i.e. that, as snow and ice cover decline further, an ever larger part of the sunlight will be absorbed by the Arctic Ocean, rather than to (a) be reflected back into space or (b) be consumed in the process of transforming ice into water. This first feedback will then be amplified by further feedbacks such as storms that can more easily develop in open water. And, as the weather becomes more extreme, stronger storms and heatwaves can be expected to hit the Arctic Ocean, causing further demise of the sea ice, resulting in more heat being absorbed by the Arctic Ocean. Thus, feedbacks can amplify each other, causing warming in the Arctic to accelerate even further. 

One of the most dangerous feedbacks is that, as the Arctic Ocean warms up further and as the Gulf Stream carries ever warmer water into the Arctic Ocean, methane can erupt from the seafloor of the Arctic Ocean in large quantities. Methane eruptions from the seafloor of the Arctic Ocean have become especially noticable over the past half year. The big danger is that this will develop into a third kind of warming, runaway global warming. 

Large amounts of methane are still entering the atmosphere over the Arctic Ocean, which contains very little hydroxyl to start with, so large abrupt releases will deplete the little hydroxyl that is there much faster than elsewhere. Furthermore, the methane will initially be highly concentrated in the atmosphere over the Arctic Ocean, and where the methane does move out of the Arctic, it could warm up the water along the track of the Gulf Stream, causing even warmer water to enter the Arctic Ocean. For years after its release, the methane will act as a powerful greenhouse gas. Unlike the albedo changes, which have the highest impact at the June Solstice when the amount of solar radiation received by the Arctic is higher than anywhere else on Earth, methane prevents heat from radiating out into space throughout the year. 

The interactive diagram below gives an overview of these three kinds of warming and the numerous feedbacks that are accelerating warming in the Arctic, from the earlier post The Biggest Story of 2013.

Hover over each kind of warming and feedback to view more details, click to go to page with further background 
Image Mapemissions cause global warmingArctic warming accelerated by soot, etc.additional warming of Gulf Stream by emissions methane releases escalatePolar vortex and jet stream weaken as Arctic warmssnow and ice decline causing less sunlight to be reflected back into spacemethane releases warm Arctic airas sea ice decline weakens vertical currents, seabed warmsStorms cause vertical mixing of wateraccelerated Arctic warming causes storms that push cold air of the Arcticextreme weather causing storms that push away sea iceextreme weather causing storms that create higher waves, breaking up the sea icestorms creating more wavy waters that absorb more sunlightextreme weather causing fires, etc.weaker polar vortex and jet stream let cold air move out of Arcticextreme weather causing warmer waterssnow and ice decline cause seismic activity that destabilizes hydratesmethane releases prevent sea ice from forming

In conclusion, the situation is dire and calls for comprehensive and effective action, as described at the Climate Plan blog.